Published by the American Geophysical Union as part of the Coastal and Estuarine Studies, Volume 35. A massive phytoplankton bloom, locally termed "brown tide", suddenly appeared in Long Island marine bays in 1985, colored the water a dark brown, decimated eelgrass beds and caused catastrophic starvation and recruitment failure of commercially important bay scallop populations. These "brown tide" blooms, caused by a very small, previously undescribed chrysophyte alga, have directly affected the estuarine environments of three northeastern American states: Rhode Island, New York and New Jersey. Other phytoplankton blooms such as "red tides" caused by dinoflagellates and "green tides" from chlorophytes as well as blue-green algae blooms have long been recognized and studied world wide, however, the unusual nature of these "brown tide" blooms caught the interest of many people. Scientists were particularly intrigued by the discovery of a previously unknown microalga which provided the opportunity to learn more about small microalgae, picoplankters, which are usually ignored due to the difficulty in identifying species. |